Some remarks on the position and shape of the neutral sheet.
Position and shape of neutral sheet in geocentric solar magnetospheric coordinate system from geomagnetic tail measurements
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Position and shape of neutral sheet in geocentric solar magnetospheric coordinate system from geomagnetic tail measurements
Component star in close binaries nonsynchronous rotation effect on limiting surface, noting difficulties associated with certain coordinate systems
Transforming Hansen lunar theory by referring satellite motion to almost ideal coordinate system, using general perturbations method
Program computes the spacecraft look angles and the slant range, which define a spherical coordinate system located in the spacecraft body. The program is designed to reduce data from the Lunar Module Missions and to output desired information.
Mathematical model and a digital computer BLITZ language programming technique computes coefficients of quadric equations describing cylinders, paraboloids, ellipsoids, or planes with any orientation to a reference system, coordinates of a vector, and coefficients of quadric surfaces which limit the surface of three-dimensional space.
Thermal plasma motion in magnetic dipole field defined by direction in coordinate system of continuity and momentum equations
Algorithm for Navier-Stokes and continuity equations used to derive curvilinear coordinate system
Data systems coordinating standards developed from experience with STADAN, discussing operating environment and administrative decisions influence on implementation
The present status (1959-60) of the ABMA early orbit determination scheme for the Juno space vehicle is described. The design of the scheme was essentially influenced by three factors: its origin centered around postflight vehicle analysis, the flexibility required for accepting varied kinds of data, and the potential of highspeed computers concentrated in ABMA's Computation Laboratory. The scheme is outlined, the tracking stations participating are shortly described, and the physical layout and computational equipment are briefly mentioned. The evaluation techniques used for the various steps of the orbit determination are discussed in detail. Appendices describe briefly the principal coordinate systems used and characteristics of the digital computer programs.
Algorithm provides for automatic input data preparation for the analysis of continuous domains in the fields of structural analysis, heat transfer, and fluid mechanics. The computer program utilizes the natural coordinate systems concept and the finite element method for data generation.
Coordinate system for synthesizing previous work on multifluid cosmologies, investigating noninteracting mixtures of multicomponent fluids
Satellite navigation method for locating Mars landmark or target point for exploration by roving vehicle located as center of coordinate system
General relativistic equations for stationary axially symmetric rotating perfect fluid in comoving coordinate system
Lumped parameter simulation model for flexible turbine rotor dynamics in nonspinning coordinate system, discussing bearing constraints modeling methods and eigenanalysis applicability
Geophysical cartesian coordinate system transformation, using vector-matrix formalism
FORTRAN 4 program for use on IBM 7094 computer for calculating temperature field of shaft seals is described. Shaft seals are composed of basically axisymmetric bodies. Cylindrical coordinate system is used as basis for analysis. Program is quite general and can be applied to variety of axisymmetric body problems.
The dose rate in a rotationally-symmetric radiation field near a space power reactor is assumed to be inversely proportional to separation distance squared and directly proportional either to a constant or a constant times the sine-cubed of a polar angle. Constant velocity motion is examined in both cases in both two and three dimensional geometries. The two dimensional geometry occurs when the line of motion and the field axis of symmetry are co-planar. The dose integral in the sine-cubed region may be integrated directly, but a more useful form is obtained after a change of variable. A coordinate system rotation greatly simplifies the results. The three dimensional problem is integrated after a change of variable. Finally, tables of normalized functions are presented and discussed.